Standard

Current-controlled sedimentation in the north-western Weddell Sea. / Leitchenkov, G.L.; Minina, V.V.; Guseva, Yu.B.

в: ПРОБЛЕМЫ АРКТИКИ И АНТАРКТИКИ, № 67 (4), 09.12.2021, стр. 382-393.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Leitchenkov, GL, Minina, VV & Guseva, YB 2021, 'Current-controlled sedimentation in the north-western Weddell Sea', ПРОБЛЕМЫ АРКТИКИ И АНТАРКТИКИ, № 67 (4), стр. 382-393. https://doi.org/10.30758/0555-2648-2021-67-4-382-393

APA

Leitchenkov, G. L., Minina, V. V., & Guseva, Y. B. (2021). Current-controlled sedimentation in the north-western Weddell Sea. ПРОБЛЕМЫ АРКТИКИ И АНТАРКТИКИ, (67 (4)), 382-393. https://doi.org/10.30758/0555-2648-2021-67-4-382-393

Vancouver

Leitchenkov GL, Minina VV, Guseva YB. Current-controlled sedimentation in the north-western Weddell Sea. ПРОБЛЕМЫ АРКТИКИ И АНТАРКТИКИ. 2021 Дек. 9;(67 (4)):382-393. https://doi.org/10.30758/0555-2648-2021-67-4-382-393

Author

Leitchenkov, G.L. ; Minina, V.V. ; Guseva, Yu.B. / Current-controlled sedimentation in the north-western Weddell Sea. в: ПРОБЛЕМЫ АРКТИКИ И АНТАРКТИКИ. 2021 ; № 67 (4). стр. 382-393.

BibTeX

@article{74c7b71164a24ffca2a760ddcf462f48,
title = "Current-controlled sedimentation in the north-western Weddell Sea",
abstract = "The sedimentary basins of the north-western Weddell Sea are characterized by a variety of contourite drifts. This study is aimed at their identification, spatial mapping and temporal evolution and based on the integration of a large amount of seismic data collected by different countries including the recent data of the Russian Antarctic Expedition. Most of the drifts in the region being studied are classified as separated, confined, plastered or sheeted. The chain of sediment wave fields is mapped in the western and northern Powell Basin. The earliest contourite drifts started to form in the Early Miocene or, possibly, in the Late Oligocene. The changes in the depositional pattern in the Middle Miocene and then in the Late Pliocene are thought to have resulted from successive intensification of the bottom currents. ",
keywords = "ANTARCTIC, BOTTOM CURRENTS, CONTOURITE DRIFTS, JANE BASIN, POWELL BASIN, SEISMIC RESEARCH, SEISMIC STRATIGRAPHY, WEDDELL SEA",
author = "G.L. Leitchenkov and V.V. Minina and Yu.B. Guseva",
note = "Leitchenkov L.G., Minina V.V., Guseva Yu.B. Current-controlled sedimentation in the north-western Weddell Sea. Arctic and Antarctic Research. 2021;67(4):382-393. https://doi.org/10.30758/0555-2648-2021-67-4-382-393",
year = "2021",
month = dec,
day = "9",
doi = "10.30758/0555-2648-2021-67-4-382-393",
language = "English",
pages = "382--393",
journal = "ПРОБЛЕМЫ АРКТИКИ И АНТАРКТИКИ",
issn = "0555-2648",
publisher = "Арктический и антарктический НИИ",
number = "67 (4)",

}

RIS

TY - JOUR

T1 - Current-controlled sedimentation in the north-western Weddell Sea

AU - Leitchenkov, G.L.

AU - Minina, V.V.

AU - Guseva, Yu.B.

N1 - Leitchenkov L.G., Minina V.V., Guseva Yu.B. Current-controlled sedimentation in the north-western Weddell Sea. Arctic and Antarctic Research. 2021;67(4):382-393. https://doi.org/10.30758/0555-2648-2021-67-4-382-393

PY - 2021/12/9

Y1 - 2021/12/9

N2 - The sedimentary basins of the north-western Weddell Sea are characterized by a variety of contourite drifts. This study is aimed at their identification, spatial mapping and temporal evolution and based on the integration of a large amount of seismic data collected by different countries including the recent data of the Russian Antarctic Expedition. Most of the drifts in the region being studied are classified as separated, confined, plastered or sheeted. The chain of sediment wave fields is mapped in the western and northern Powell Basin. The earliest contourite drifts started to form in the Early Miocene or, possibly, in the Late Oligocene. The changes in the depositional pattern in the Middle Miocene and then in the Late Pliocene are thought to have resulted from successive intensification of the bottom currents.

AB - The sedimentary basins of the north-western Weddell Sea are characterized by a variety of contourite drifts. This study is aimed at their identification, spatial mapping and temporal evolution and based on the integration of a large amount of seismic data collected by different countries including the recent data of the Russian Antarctic Expedition. Most of the drifts in the region being studied are classified as separated, confined, plastered or sheeted. The chain of sediment wave fields is mapped in the western and northern Powell Basin. The earliest contourite drifts started to form in the Early Miocene or, possibly, in the Late Oligocene. The changes in the depositional pattern in the Middle Miocene and then in the Late Pliocene are thought to have resulted from successive intensification of the bottom currents.

KW - ANTARCTIC

KW - BOTTOM CURRENTS

KW - CONTOURITE DRIFTS

KW - JANE BASIN

KW - POWELL BASIN

KW - SEISMIC RESEARCH

KW - SEISMIC STRATIGRAPHY

KW - WEDDELL SEA

U2 - 10.30758/0555-2648-2021-67-4-382-393

DO - 10.30758/0555-2648-2021-67-4-382-393

M3 - Article

SP - 382

EP - 393

JO - ПРОБЛЕМЫ АРКТИКИ И АНТАРКТИКИ

JF - ПРОБЛЕМЫ АРКТИКИ И АНТАРКТИКИ

SN - 0555-2648

IS - 67 (4)

ER -

ID: 89363645